The Middle Caradoc Facies and Faunal Turnover in the Late Ordovician Baltoscandian palaeobasin

A Late Ordovician episode of remarkable biotic, climatic, sea level and facies changes, named here as the Middle Caradoc Facies and Faunal Turnover, took place in the Baltoscandian area. This paper presents an integrated overview of these changes in the critical middle Caradoc interval. Data are given on carbonate rock composition, distribution and grain-size composition of the siliciclastic material and the carbon isotopic composition of whole-rock carbonates in cores of Estonia and Sweden.

The Middle Caradoc Facies and Faunal Turnover can be described as a succession of related environmental changes. The turnover began with a positive excursion in carbonate δ¹³C and continued with sea level changes that led to a sedimentary hiatus on the shelf and a change from carbonate-dominated to siliciclastic-dominated sedimentation in the basin. The turnover ended with an extinction event and associated microfaunal crisis.

The middle Caradoc turnover in Baltoscandia is comparable to a similar succession of changes in North America. The turnover affected two palaeocontinents, and reflects a widespread, possibly global environmental change. Onset of glaciation on Gondwana and/or increased orogenic activity might have initiated the changes in ocean circulation and led to the initial carbon isotope excursion. The following sea level rise and faunal changes affected several different continents.     

Effect of CO2 on carbonic anhydrase in Avena sativa and Zea mays

In leaves of Zea mays kept in air with reduced or increased CO₂, the level of carbonic anhydrase is reduced or increased respectively. In Avena sativa an opposite effect of pCO₂ is observed. In both cases the enzyme activity rapidly reached normal values when the plants were transferred back to normal atmosphere.     

万峰湖水库溶解性无机碳来源及时空变异特征

溶解性无机碳(DIC)的通量和形式在水生态系统的生物地球化学循环中起关键作用,是碳收支的重要组成部分。通过分析万峰湖水库库区水体理化参数、DIC和稳定碳同位素(δ¹³C_DIC)特征,揭示了DIC的行为和来源。结果表明: 1)在表水层,整个库区pH变化较保守,均呈弱碱性。硝酸盐氮(NO₃^--N)有最大变异系数,具有高度的时空变异性。由于稀释效应的存在,电导率(EC)、二氧化碳分压(pCO₂)和DIC的最低值均出现在夏季高径流量阶段。在水柱面上,夏季氧化还原电位(Eh)和NO₃^--N随水深增加无显著变化,其余指标均变化明显,且在温跃层变异程度最大。两季节的水温(T)、pH和Eh均随水深增加而降低,pCO₂则与之相反。EC、总碱度(TA)和DIC在夏季随水深增加而降低,冬季变化梯度较小。两季节的DIC与pH、Eh呈负相关,与EC、pCO₂呈正相关。2)夏季DIC为2.66～4.9 mmol·L^-1,而冬季为3.38～4.52 mmol·L^-1。水体热分层期间,DIC和δ¹³C_DIC在温跃层的变化梯度最大,DIC与δ¹³C_DIC在夏季表水层呈正相关。两个季节水柱面上及冬季表水层的DIC和δ¹³C_DIC均呈负相关,但冬季DIC和δ¹³C_DIC值随水深变化趋势不明显。3)夏季δ¹³C_DIC较高,为-7.71‰～-1.38‰,表明碳酸盐矿物的溶解占优势。冬季δ¹³C_DIC为-16.93‰～-9.44‰,显著低于夏季且范围更宽,生物源CO₂的输入和有机质矿化是主要来源。δ¹³C_DIC在不同季节和水深均差异显著,一方面是碳的来源不同;另一方面归因于碳来源的相对贡献比例的变化。     

Differences in HPRT mutant frequency among middle-aged Flemish women in association with area of residence and blood lead levels

Biomarkers were measured in residents of Wilrijk and Hoboken, industrial suburbs of the city of Antwerp, and of Peer, a rural municipality in Flanders, Belgium. Persons with known occupational exposures to toxic compounds or commuting over long distances were excluded. Here, we report the hypoxanthine phosphoribosyltransferase gene (HPRT) variant frequencies for 99 non-smoking women aged 50-65 years. HPRT values above the detection limit (V_fpos values) were observed for 43 subjects (21 from Peer, 22 from Antwerp). The median (10th to 90th percentiles) HPRT variant frequency (V_fpos) in peripheral lymphocytes was 9.59 (3.44-56.99) for Peer and 3.57 (1.57-13.96) for Antwerp. The V_fpos value was significantly higher in Peer than in Antwerp, both in terms of crude data (p=0.011) and after correction for age, level of education, smoking status, serum level of selenium and body mass index through analysis of covariance (p=0.011). For the total study population, serum lead concentration showed a non-significant positive correlation with lnV_fpos. In addition, subjects with a blood lead concentration above the median tended to have higher V_fpos values (9.45×10^-6 for 'high' group versus 5.21×10^-6 for 'low' group; p=0.077 after correction for confounding). Subjects with a serum selenium level above the median tended to have lower V_fpos values (4.99×10^-6 for 'high' group versus 9.83×10^-6 for 'low' group; p=0.051 after correction for confounding). These data are consistent with an indirect genotoxic effect of lead and with an antimutagenic effect of selenium.     

The Ordovician Biodiversification: revolution in the oceanic trophic chain

The Early Palaeozoic phytoplankton (acritarch) radiation paralleled a long-term increase in sea level between the Early Cambrian and the Late Ordovician. In the Late Cambrian, after the SPICE δ¹³C_carb excursion, acritarchs underwent a major change in morphological disparity and their taxonomical diversity increased to reach highest values during the Middle Ordovician (Darriwilian). This highest phytoplankton diversity of the Palaeozoic was possibly the result of palaeogeography (greatest continental dispersal) and major orogenic and volcanic activity, which provided maximum ecospace and large amounts of nutrients. With its warm climate and high atmospheric CO₂ levels, the Ordovician was similar to the Cretaceous: a period when phytoplankton diversity was at its maximum during the Mesozoic. With increased phytoplankton availability in the Late Cambrian and Ordovician a radiation of zooplanktonic organisms took place at the same time as a major diversification of suspension feeders. In addition, planktotrophy originated in invertebrate larvae during the Late Cambrian–Early Ordovician. These important changes in the trophic chain can be considered as a major palaeoecological revolution (part of the rise of the Palaeozoic Evolutionary Fauna of Sepkoski). There is now sufficient evidence that this trophic chain revolution was related to the diversification of the phytoplankton, of which the organic-walled fraction is partly preserved.     

Influence de l'oxygene sur les transferts d'electrons de la photosynthese. I. Influence de diverses concentrations d'oxygene sur quel ques reactions de Hill

Influence of oxygen on the electron transfers of photosynthesis. I. Influence of some oxygen concentrations on some Hill reactions

The influence of O₂ concentrations on the Hill reactions in the presence of p-benzoquinone, ferricyanide, NADP⁺, NADP⁺ plus ferredoxin has been studied with isolated spinach chloroplasts.

Because of the partial reoxidation of the hydroquinone, which is depending upon the O₂ concentration, it does not seem possible to localize a site of action for O₂.

With ferricyanide the influence of O₂ is weak. However, the rate of ferricyanide reduction is increased in the presence of O₂. The observed stimulation is greater for 21% O₂ than for 70% O₂. Bicarbonate stimulates the ferricyanide reduction and decreases the stimulating effect of 21% O₂.

O₂ decreases the rate of NADP⁺ reduction. Ferredoxin as well as bicarbonate stimulate the NADP⁺ reduction and reduce the O₂ inhibition.

These results seem to indicate that O₂ may enter the electron transport chain at a site situated near Photosystem I and before the ferredoxin's site.

The inhibitory effect of O₂ on the Hill reactions with p-benzoquinone and NADP⁺ is depending upon the plants' growth conditions. It is greater with plants grown under weak light.     

Sensitivity of a dynamic global vegetation model to climate and atmospheric CO2

The equilibrium carbon storage capacity of the terrestrial biosphere has been investigated by running the Lund–Potsdam–Jena Dynamic Global Vegetation Model to equilibrium for a range of CO₂ concentrations and idealized climate states. Local climate is defined by the combination of an observation-based climatology and perturbation patterns derived from a 4 × CO₂ warming simulations, which are linearly scaled to global mean temperature deviations, Δ T _glob. Global carbon storage remains close to its optimum for Δ T _glob in the range of ±3°C in simulations with constant atmospheric CO₂. The magnitude of the carbon loss to the atmosphere per unit change in global average surface temperature shows a pronounced nonlinear threshold behavior. About twice as much carbon is lost per degree warming for Δ T _glob above 3°C than for present climate. Tropical, temperate, and boreal trees spread poleward with global warming. Vegetation dynamics govern the distribution of soil carbon storage and turnover in the climate space. For cold climate conditions, the global average decomposition rate of litter and soil decreases with warming, despite local increases in turnover rates. This result is not compatible with the assumption, commonly made in global box models, that soil turnover increases exponentially with global average surface temperature, over a wide temperature range.     

Conodontophorid biodiversification during the Ordovician in South China

Wu, R., Stouge, S. & Wang, Z. 2012: Conodontophorid biodiversification during the Ordovician in South China. Lethaia, Vol. 45, pp. 432–442. Analysis of the Ordovician conodontophorid diversity pattern for South China using normalized and total diversity measures reveals that diversity peaks occurred in the mid‐Tremadocian, mid‐late Floian, early Dapingian and mid‐Darriwilian periods. The conodontophorids radiated during the Floian, maintaining relatively high diversity into the early part of the Middle Ordovician until a significant diversity decrease occurred in the late Dapingian. A relatively low diversity level prevailed in the Late Ordovician. Three diversification intervals based on origination, extinction and turnover rates have been identified i.e. (1) Tremadocian to mid‐late Floian, (2) early Dapingian and (3) late Dapingian to early Darriwilian. Diversity curves for conodontophorids, brachiopods, graptolites, acritarchs and trilobites from South China are comparable during the Early Ordovician, although differences are apparent in the Middle and Late Ordovician. In South China, conodontophorid diversity reacted primarily to sea‐level changes during the Early and Middle Ordovician, when the peak of this biodiversification generally coincided with a transgression. Climate changes – especially the global cooling that occurred during the Late Ordovician glaciation – and sea‐water chemistry were also important controlling factors. □Biodiversification, conodonts, Ordovician, South China.     

A quantitative study of spermatogonial multiplication and stem cell renewal in the C3H/101 F1 hybrid mouse

In whole mounts of seminiferous tubules of C3H/101 F₁ hybrid mice, spermatogonia were counted in various stages of the epithelial cycle. Furthermore, the total number of Sertoli cells per testis was estimated using the disector method. Subsequently, estimates were made of the total numbers of the different spermatogonial cell populations per testis.

The results of the cell counts indicate that the undifferentiated spermatogonia are actively proliferating from stage XI until stage IV. Three divisions of the undifferentiated spermatogonia are needed to obtain the number of A₁ plus undifferentiated spermatogonia produced each epithelial cycle. Around stage VIII almost two-thirds of the A_pr and all of the A_al spermatogonia differentiate into A₁ spermatogonia. It was estimated that there are 2.5 × 10⁶ differentiating spermatogonia and 3.3 × 10⁵ undifferentiated spermatogonia per testis. There are about 35,000 stem cells per testis, constituting about 0.03% of all germ cells in the testis. It is concluded that the undifferentiated spermatogonia, including the stem cells, actively proliferate during about 50% of the epithelial cycle.     

施氮和大气CO2浓度升高对小麦旗叶光合电子传递和分配的影响

采用开顶式气室盆栽培养小麦,设计2个大气CO₂浓度（正常：400 μmol·mol^-1;高：760 μmol·mol^-1）、2个氮素水平（0和200 mg·kg^-1土）的组合处理,通过测定小麦抽穗期旗叶氮素和叶绿素浓度、光合速率（P_n）-胞间CO₂浓度（C_i）响应曲线及荧光动力学参数,来测算小麦叶片光合电子传递速率等,研究了高大气CO₂浓度下施氮对小麦旗叶光合能量分配的影响.结果表明：与正常大气CO₂浓度相比,高大气CO₂浓度下小麦叶片氮浓度和叶绿素浓度降低,高氮处理的小麦叶片叶绿素a/b升高.施氮后小麦叶片PSⅡ最大光化学效率（F_v/F_m）、PSⅡ反应中心最大量子产额（F_v′/F_m′）、PSⅡ反应中心的开放比例（q_p）和PSⅡ反应中心实际光化学效率（Φ_PSⅡ）在大气CO₂浓度升高后无明显变化,虽然叶片非光化学猝灭系数（NPQ）显著降低,但PSⅡ总电子传递速率（J_F）无明显增加;不施氮处理的F_v′/F_m′、Φ_PSⅡ和NPQ在高大气CO₂浓度下显著降低,尽管F_v/F_m和q_P无明显变化,J_F仍显著下降.施氮后小麦叶片J_F增加,参与光化学反应的非环式电子流传递速率(J_C)明显升高.大气CO₂浓度升高使参与光呼吸的非环式电子流传递速率(J₀)、Rubisco氧化速率（V₀）、光合电子的光呼吸/光化学传递速率比（J₀/J_C）和Rubisco氧化/羧化比（V₀/V_C）降低,但使J_C和Rubisco羧化速率（V_C）增加.因此,高大气CO₂浓度下小麦叶片氮浓度和叶绿素浓度降低,而增施氮素使通过PSⅡ反应中心的电子流速率显著增加,促进了光合电子流向光化学方向的传递,使更多的电子进入Rubisco羧化过程,P_n显著升高.     

Arabia–Eurasia collision and the forcing of mid-Cenozoic global cooling

The end of the Eocene greenhouse world was the most dramatic phase in the long-term cooling trend of the Cenozoic Era. Here we show that the Arabia–Eurasia collision and the closure of the Tethys ocean gateway began in the Late Eocene at ~ 35 Ma, up to 25 million years earlier than in many reconstructions. We suggest that global cooling was forced by processes associated with the initial collision that reduced atmospheric CO₂. These are: 1) waning volcanism across southwest Asia; 2) increased organic carbon storage in Paratethyan basins (e.g. Black Sea and South Caspian); 3) increased silicate weathering in the collision zone and, 4) a shift towards modern patterns of ocean currents, associated with increased vigour in circulation and organic productivity.     

CO2 levels in the Late Palaeozoic and Mesozoic atmosphere from soil carbonate and organic matter, Satpura basin, Central India

A number of calcic palaeosols have been identified within the fluvial deposits of the Motur (Permian), the Denwa (Triassic), the Bagra (Jurassic) and the Lameta (Cretaceous) Formations of the Satpura sedimentary succession, Central India. These palaeosols show accumulation of pedogenic carbonates in rhizocretions and glaebules. The carbon isotopic compositions of these carbonates and the coexisting soil organic matters are used to determine the isotopic composition and the partial pressure of atmospheric CO₂ using the CO₂ palaeobarometer developed by Cerling [Am. J. Sci., 291 (1991) 377]. It is seen that the atmospheric CO₂ level increased by a factor of 8 from the Permian to the Jurassic and declined again during the Cretaceous. The nature of the changes agrees with the result of the CO₂ evolution model of Berner (GEOCARB II) but the magnitude of the CO₂ increase in the Middle Jurassic and the Late Cretaceous was higher than the predicted value. Degassing of Earth's interior due to rapid break-up of the Gondwana landmass during the Triassic and Jurassic period could have caused the rapid CO₂ increase.     

Characterization of phospholipase A2 and acyltransferase activities in squid (Loligo pealei) axoplasm: comparison with enzyme activities in other neural tissues, axolemma and axoplasmic subfractions.

Phospholipase A₂ and acyltransferase were assayed and characterized in pure axoplasm and neural tissues of squid. Intracellular phospholipase A₂ activity was highest in giant fiber lobe and axoplasm, followed by homogenates from retinal fibers, optic lobe and fin nerve. In most preparations, exogenous calcium (5 mM) caused a slight stimulation of activity. EGTA (2 mM) was somewhat inhibitory, indicating that low levels of endogenous calcium may be required for optimum activity. Phospholipase A₂ was inhibited by 0.1 mM p-bromophenacylbromide, and was completely inactivated following heating.

The level of acylCoA: lysophosphatidylcholine acyltransferase activity was higher in axoplasm and giant fiber lobe than in other neural tissues of the squid. K_m (apparent) and V_max (apparent) for oleoyl-CoA and lysophosphatidylcholine were quite similar for axoplasm and giant fiber lobe enzyme preparations. Acyltransferase activity was inactivated by heat treatment, and greatly inhibited by 0.2 mM p-chloromercuribenzoate, and to a lesser extent by 20 mM N-ethylmaleimide.

Phospholipase A₂ activity was present in fractions enriched in axolemmal membranes (separated from squid retinal fibers and garfish olfactory nerve) from both tissues, and it was also highly concentrated in vesicles derived from squid axoplasm. In all three preparations, phospholipase A₂ activity was stimulated by Ca⁺⁺ (5 mM) and inhibited by EGTA (2 mM). In addition, axoplasmic cytosol (114,000 g supernatant) retained a substantial portion of a Ca⁺⁺-independent phospholipase A₂, active in the presence of 2 mM EGTA. Acyltransferase activity was present at high content in both axolemma membrane rich fractions, and among subaxoplasmic fractions and axoplasmic vesicles.     

Photosynthetic carbon metabolism in Panicum milioides, a C3-C4 intermediate species: Evidence for a limited C4 dicarboxylic acid pathway of photosynthesis

Panicum milioides, a naturally occurring species with C₄-like Kranz leaf anatomy, is intermediate between C₃ and C₄ plants with respect to photorespiration and the associated oxygen inhibition of photosynthesis. This paper presents direct evidence for a limited degree of C₄ photosynthesis in this C₃-C₄ intermediate species based on:

1. (a) the appearance of 24% of the total ¹⁴C fixed following 4 s photosynthesis in ¹⁴CO₂-air by excised leaves in malate and aspartate and the complete transfer of label from the C₄ acids to Calvin cycle intermediates within a 15 s chase in ¹²CO₂-air;

2. (b) pyruvate- or alanine-enhanced light-dependent CO₂ fixation and pyruvate stimulation of oxaloacetate- or 3-phosphoglycerate-dependent O₂ evolution by illuminated mesophyll protoplasts, but not bundle sheath strands; and

3. (c) NAD-malic enzyme-dependent decarboxylation of C₄ acids at the C-4 carboxyl position, C₄ acid-dependent O₂ evolution, and ¹⁴CO₂ donation from [4-¹⁴C]C₄ acids to Calvin cycle intermediates during photosynthesis by bundle sheath strands, but not mesophyll protoplasts.

However, P. milioides differs from C₄ plants in that the activity of the C₄ cycle enzymes is only 15 to 30% of a C₄ Panicum species and the Calvin cycle and phosphoenolpyruvate carboxylase are present in both cell types. From these and related studies (Rathnam, C.K.M. and Chollet, R. (1979) Arch. Biochem. Biophys. 193, 346–354; (1978) Biochem. Biophys. Res. Commun. 85, 801–808) we conclude that reduced photorespiration in P. milioides is due to a limited degree of NAD-malic enzyme-type C₄ photosynthesis permitting an increase in pCO₂ at the site of bundle sheath, but not mesophyll, ribulosebisphosphate carboxylase-oxygenase.     

Etude des mutants chlorate-resistants d'escherichia coli K12. IV. Isolement, purification et etude de la nitrate-reductase reconstituee In vitro par complementation

Study on chlorate-resistants mutants of Escherichia coli K12. IV. Isolation, purification and study of nitrate-reductase restored in vitro by complementation

By mixing the cell-free extracts of the two mutants chl A⁻ and chl B⁻ of Escherichia coli K12, previously freed from particle membranes, we achieved restoration of nitrate reductase activity. The activity is restored first in a soluble form, then in a particulate form. This mechanism is called “complementation”. In the soluble state, the purified enzyme reduces NO₃⁻ and ClO₃⁻, using reduced benzyl viologen or FMNH₂ as electron donors. It is sensitive to KCN, NaN₃, p-hydroxymercuribenzoate (1 mM) and N-ethylmaleimide (0.1 mM)

The soluble form is sensitive neither to phospholipase C, nor to 2-n-heptyl-4-hydroxyquinoline-N-oxide; it associates with phospholipids and cytochrome b₁ to form particles in which nitrate reductase activity is no longer sensitive to ethyl N-maleimide and p-hydroxymercuribenzoate, but, conversely, becomes sensitive to 2-n-heptyl-4-hydroxyquinoline-N-oxide.

These results clearly demonstrate that it is possible to study the mechanism of integration of the enzyme leading to active membranes particles without any previous solubilisation of the original material.     

Changes in phenylalanine ammonia-lyase levels in excised potato tuber tissue: effects of the gaseous environment and desensitization to cinnamate repression by in situ pre-incubation

Abstract. The rise in phenylalanine ammonia-lyase (PAL) activity following excision of potato tuber discs is antagonized by increasing partial pressures of CO₂ This inhibition is potentiated by depleting the atmospheric ethylene level. We suggest that the previously observed suppression of PAL appearance by in situ incubation of excised discs in reassembled tubers may be related to an internal atmosphere relatively rich in CO₂ and of low ethylene content. The transition to an oscillatory time course of PAL activity that follows transfer of discs from in situ incubation to air appears to be accompanied by the development of enzyme activity becoming desensitized to repression by exogenous cinnamate. The concentration dependence of cinnamate uptake is not significantly altered by in situ pre-incubation of tuber discs.     

不同无机碳转运基因型蓝藻对环境CO2变化的响应

为了探究不同无机碳(Ci)转运基因型蓝藻与湖泊水体pH变化的关系,文章优化了水体中不同无机碳转运基因型蓝藻相对丰度的检测方法,测定了太湖、滇池及武汉市18个湖泊中具有不同无机碳(Ci)转运基因型蓝藻的相对丰度,并结合水体pH进行分析。结果发现,在所有湖泊中均存在bicA株、sbtA株及bicA+sbtA株,其中sbtA株分布最为广泛;随着水体中pH升高, sbtA株优势度随之增加。为了进一步解析不同Ci转运基因型蓝藻对CO₂浓度变化的响应,研究了室内纯培养条件下bicA株、sbtA株及bicA+sbtA株分别在高浓度(1000 ppm)和低浓度(100 ppm)CO₂下的竞争。结果显示,在低Ci水平下sbtA株具有明显竞争优势,而在高Ci水平下bicA株占据了优势地位。上述研究表明随着CO₂浓度的上升,水华蓝藻中bicA株会具有竞争优势。大气CO₂浓度上升可能会显著影响水华蓝藻的群落组成。     

全球变化主要过程对海滨生态系统生物入侵的影响

作为海陆交错带的海滨生态系统是海洋与陆地的过渡带, 是承受全球变化及其引起海平面上升等影响最为前沿、最为重要的缓冲带, 同时又是人类活动极为频繁和强烈的地带, 因此海滨生态系统是生物入侵的高发区之一。本文在分析海滨生态系统生物入侵现状的基础上, 分析了CO₂升高、海平面上升和富营养化等全球变化过程对海滨生态系统生物入侵的影响: CO₂浓度上升改变了入侵种的竞争态势, 海平面上升调整了入侵种的空间分布格局, 而富营养化为外来入侵种的进一步拓展提供了动力。为了深入揭示全球变化对海滨生态系统生物入侵过程的潜在影响, 很有必要在阐明单因子作用机制与过程的基础上加强与其他组分的交互作用研究, 以及中、长时间尺度上的动态分析。与此同时, 生物入侵导致的海滨生态系统变化对全球变化相关过程的反馈作用研究也具有极其重要的意义。     

Metal carbonyls of telluroether formed by the oxygen atom transfer reaction to M(CO)6 (M = Mo, W) in the presence of (p-CH3OC6H4)2TeO and relative kinetic investigation

A new synthetic process is reported for the preparation of two substituted metal carbonyls, (p-CH₃OC₆H₄)₂TeM(CO)₅ (M = Mo, W). In the presence of (p-CH₃OC₆H₄)₂TeO as O atom transfer reagent in tetrahydrofuran solvent, a CO ligand is replaced by telluroether when M(CO)₆ (M = Mo, W) is reacted with (p-CH₃OC₆H₄)₂TeO under very mild experimental conditions (r.t.). The products were characterized by elemental analysis, mass, IR and ¹H NMR spectroscopies. The spectra suggest that the coordination geometry is distorted from a regular octahedral structure due to an asymmetrical bulky telluroether ligand on the metal atom. Kinetics of these reactions of M(CO)₆ with (p-CH₃OC₆H₄)₂TeO show the reactions are first order in the concentration of M(CO)₆ and of Te oxide. The rates of reaction decrease in the order W(CO)₆>Mo(CO)₆>Cr(CO)₆, and the results obtained are discussed in term of a presumed mechanism.     

Interactions between increasing CO2 concentration and temperature on plant growth

The global environment is changing with increasing temperature and atmospheric carbon dioxide concentration, [CO₂]. Because these two factors are concomitant, and the global [CO₂] rise will affect all biomes across the full global range of temperatures, it is essential to review the theory and observations on effects of temperature and [CO₂] interactions on plant carbon balance, growth, development, biomass accumulation and yield. Although there are sound theoretical reasons for expecting a larger stimulation of net CO₂ assimilation rates by increased [CO₂] at higher temperatures, this does not necessarily mean that the pattern of biomass and yield responses to increasing [CO₂] and temperature is determined by this response. This paper reviews the interactions between the effects of [CO₂] and temperature on plants. There is little unequivocal evidence for large differences in response to [CO₂] at different temperatures, as studies are confounded by the different responses of species adapted and acclimated to different temperatures, and the interspecific differences in growth form and development pattern. We conclude by stressing the importance of initiation and expansion of meristems and organs and the balance between assimilate supply and sink activity in determining the growth response to increasing [CO₂] and temperature.